THE ROCK KARSTIFICATION PROCESSES IN THE KARST AREA OF CROATIA
Main researcher
: GARAŠIĆ, MLADEN (7250) Assistants
ZMAIĆ, BOJAN (90035)
CVIJANOVIĆ, DRAGUTIN (7336)
Type of research: basic Duration from: 01/01/91. to 12/31/95. Papers on project (total): 38
Papers on project quoted in Current Contents: 17
Institution name: Institut građevinarstva Hrvatske, Zagreb (110) Department/Institute: Institute for geotechnics, Department for rock mechanics and und erground works Address: Rakušina 1 City: 10000 - Zagreb, Croatia
Communication
Phone: 385 (0)1 6136-444
Phone: 385 (0)1 534-103
Fax: 385 (0)1 534-737
Fax: 385 (0)1 533-889
E-mail: Mladen.Garasic@public.srce.hr
Summary: The karstification as the most complex and intensive
geological process today occurring in karst rocks is investigated. The
karstification can not be studied as an outside process only (atmospheric
influence and tectonic predisposition), but rather as a complex sum of
various geological factors (e.g. inverse karstification). Speleological
structures (caves and pits) are always present in karst areas and provide
an inexhaustible quantity of data used by scientists to gain a better
insight into karstification processes. This is due to the fact that the
manifestation of karstification processes is the strongest in these
structures and, unlike on the surface, this process can thoroughly be
observed and monitored. Over 6500 speleological structures have been
registered in the Croatian karst, which is in fact a locus tipicus of the
world karst areas. An additional insight into the karstification process
intensity is obtained by measuring the intensity of tectonic activity in
these structures, the ground-water aggressiveness and the influence of
discontinuity orientation in various lithostratigraphical environments. In
addition to geophysical measurements performed on specially selected
locations above speleological structures, the quantitative information on
the porosity of various karst rocks (according to their lithostratigraphic
and chronostratigraphic properties) is also defined on the basis of
ultrasonic and geomechanical testing performed in laboratory on selected
rock samples. This porosity is one of indicators of the karstification
effect. A deeper karstification is defined through seismic activities
(earthquakes and tremors). The karstified rock classification has been
made, including test maps with karstification indices that may prove quite
useful in the design and construction of civil engineering structures in
Croatian karst regions.
Research goals: As over 50% of the Croatian territory is covered by
karst relief,and considering that this karstland is a locus tipicus of
theworld karst areas, the question may be put whether the nature
andgenesis of the basic geological process present in this area
hassufficiently been investigated. This process may be investigatedon
many localities in Croatia, within a relatively small area.The main
objective of this study is to define types, intensities,influences,
modalities, indices and genesis of karstification inkarst areas. The
karstification is not just a form of tectonicmanifestation or a form of
rock deformation or weathering due toatmospheric influences, but rather a
complex relationship oflithostratigraphic, neopaleotectonic and
paleotectonic,hydrogeological, seismological, speleogeological and
otherfactors. Our aim is to prepare test maps indicating levels ofrock
karstification, which will be of great help in many areas ofscientific
research. It is expected that this study willcontribute to geological
sciences by providing better insightinto speleological structures being
the main benchmarks of paleoand neohydrogeological functions (sinkholes,
springs, estavelles,submarine springs, flow structures), by extending
knowledge onthe way ground-water influences rock karstification
(waterchemism) and by providing additional information about
theneotectonic activity and its connection with the seismicity
ofindividual areas. In the field of geophysics, significant resultsare
expected with respect to the karst-rock classification andthe ground
cavity determination. In the area of water supply, itwill be possible to
define zones of stronger or weaker rockkarstification, which is quite
interesting for water prospectingworks, as ground water occurrence also
depends on the intensityof karstification. This study will also contribute
toenvironmental protection, as more information on undergroundstreams in
karst areas will be available, and can be used toprotect environment
against various types of pollution. As acontribution to the construction
industry, more accurategeotechnical classification of karstified rocks
will beavailable, which will be quite useful in the design
andconstruction of greater structures (tunnels, transportationfacilities,
reservoirs, bridges, etc.). To facilitate analysis,all data will be
computerized.
COOPERATION - PROJECTS
Name of project
: 1-09-141 Znanstvena valorizacija krša u
Hrvatskoj Name of institution: Rudarsko geološko naftni fakultet City: 10000 - Zagreb, Croatia
COOPERATION - INSTITUTIONS
Name of institution
: Društvo za istraživanja i snimanja krških
fenomena Type of institution: Other Type of cooperation: Systematic exchange of information City: 10000 - Zagreb, Croatia
Name of institution
: Hrvatsko speleološko društvo Type of institution: Other Type of cooperation: Systematic exchange of experts City: 10000 - Zagreb, Croatia
OTHER ACHIEVEMENTS
Name
: Izložba "Hrvatska speleologija" Type of achievement: Other Authors: Mladen Garašić, Roman Ozimec, Tihomir Kovačević, Marina
Šimek Other information about the project.